Survival and behaviour of the earthworms Lumbricus rubellus and Dendrodrilus rubidus from arsenate-contaminated and non-contaminated sites

Two arsenic- and heavy metal-contaminated mine-spoil sites, at Carrock Fell, Cumbria and Devon Great Consols Mine, Devon, were found to support populations of the earthworms Lumbricus rubellus Hoffmeister and Dendrodrilus rubidus (Savigny). L. rubellus and D. rubidus collected from the Devon site and an uncontaminated site were kept for 28 days in uncontaminated soil and in soil containing sodium arsenate (494 mg As kg^-1). The state of the specimens was recorded every 7 days using a semi-quantitative assessment of earthworm health (condition index, C. I.). The C. I. remained high for all specimens except those of L. rubellus and D. rubidus from uncontaminated sites, which displayed 60 and 10% mortality, respectively. L. rubellus collected from the Carrock Fell site, and L. rubellus and D. rubidus from an uncontaminated site, burrowed as rapidly into soil containing up to 1235 mg As kg^-1 in the form of sodium arsenate as into uncontaminated soil when placed on the soil surface. When earthworms were allowed a choice between uncontaminated soil and soil contaminated with sodium arsenate in concentrations of up to 1235 mg As kg^-1, the threshold concentration for avoidance of contaminated soil was lower for L. rubellus and D. rubidus from uncontaminated soil than for specimens from contaminated soil. There was no significant effect of pH on soil discrimination. The LC₅₀ concentration of As for L. rubellus from Devon Great Consols was significantly higher (P < 0.001) than for L. rubellus from the uncontaminated site: 1510 and 96 mg As kg^-1, respectively. © 2001 Elsevier Science Ltd. All rights reserved.

Copper- and arsenate-induced oxidative stress in Holcus lanatus L. clones with differential sensitivity

The biochemical responses of Holcus lanatus L. to copper and arsenate exposure were investigated in arsenate-tolerant and -non-tolerant plants from uncontaminated and arsenic/copper-contaminated sites. Increases in lipid peroxidation, superoxide dismutase (SOD) activity and phytochelatin (PC) production were correlated with increasing copper and arsenate exposure. In addition, significant differences in biochemical responses were observed between arsenate-tolerant and -non-tolerant plants. Copper and arsenate exposure led to the production of reactive oxygen species, resulting in significant lipid peroxidation in non-tolerant plants. However, SOD activity was suppressed upon metal exposure, possibly due to interference with metallo-enzymes. It was concluded that in non-tolerant plants, rapid arsenate influx resulted in PC production, glutathione depletion and lipid peroxidation. This process would also occur in tolerant plants, but by decreasing the rate of influx, they were able to maintain their constitutive functions, detoxify the metals though PC production and quench reactive oxygen species by SOD activity.

Genetic diversity of root-associated fungal endophytes from Calluna vulgaris at contrasting field sites

A total of 107 putative ericoid mycorrhizal endophytes were isolated from hair roots of Calluna vulgaris from two abandoned arsenic/copper mine sites and a natural heathland site in southwest England. The endophytes were initially grouped as 14 RFLP types, based on the results of ITS-RFLP analysis using the restriction endonucleases Hinf I, Rsa I and Hae III. ITS sequences were obtained for representative isolates from each RFLP type and compared phylogenetically with sequences for known ericoid mycorrhizal endophytes and selected ascomycetes. The majority of endophyte isolates (62-92%) from each site were identified as Hymenoscyphus ericae, but a number of other less common mycorrhizal RFLP types were also identified, all of which appear to have strong affinities with the order Leotiales. None of the less common RFLP types was isolated from C. vulgaris at more than one field site. Neighbour-joining analysis indicated similarities between the endophytes from C. vulgaris and mycorrhizal endophytes isolated from other Ericaceae and Epacridaceae hosts in North America and Australia.

Edaphic factors affecting the toxicity and accumulation of arsenate in the earthworm Lumbricus terrestris

The toxicity and accumulation of arsenate was determined in the earthworm Lumbricus terrestris in soil from different layers of a forest profile. Toxicity increased fourfold between 2 and 10 d. Edaphic factors (pH, soil organic matter, and depth in soil profile) also affected toxicity with a three fold decrease in the concentration that causes 50% mortality with increasing depth in soil (from 0-70 mm to 500-700 mm). In a 4-d exposure study, there was no evidence of arsenic bioconcentration in earthworm tissue, although bioaccumulation was occurring. There was a considerable difference in tissue residues between living and dead earthworms, with dead worms having higher concentrations. This difference was dependent on both soil arsenate concentration and on soil type. Over a wide range of soil arsenate concentrations, earthworm arsenic residues are homeostatically maintained in living worms, but this homeostasis breaks down during death. Alternatively, equilibration with soil residues may occur via accumulation after death. In long-term accumulation studies in soils dosed with a sublethal arsenate concentration (40 μg/g dry weight), bioconcentration of arsenate did not occur until day 12, after which earthworm concentrations rose steadily above the soil concentration, with residues in worms three fold higher than soil concentrations by the termination of the study (23 d). This bioconcentration only occurred in depurated worms over the time period of the study. Initially, depurated worms had lower arsenic concentrations than undepurated until tissue concentrations were equivalent to the soil concentration. Once tissue concentration was greater than soil concentration, depurated worms had higher arsenic residues than undepurated.

Biomass allocation, phosphorus nutrition and vesicular-arbuscular mycorrhizal infection in clones of Yorkshire Fog, Holcus lanatus L. (Poaceae) that differ in their phosphate uptake kinetics and tolerance to arsenate

Biomass and phosphorus allocation were determined in arsenate tolerant and non-tolerant clones of the grass Holcus lanatus L. in both solution culture and in soil. Arsenate is a phosphate analogue and is taken up by the phosphate uptake system. Tolerance to arsenate in this grass is achieved by suppression of arsenate (and phosphate) influx. When clones differing in their arsenate tolerance were grown in solution culture with a range of phosphate levels, a tolerant clone did not fare as well as a non-tolerant at low levels of phosphate nutrition in that it had reduced shoot biomass production, increased biomass allocation to the roots and lower shoot phosphorus concentration. At a higher level of phosphate nutrition there was little or no difference in these parameters, suggesting that differences at lower levels of phosphate nutrition were due solely to differences in the rates of phosphate accumulation. In experiments in sterile soil (potting compost) the situation was more complicated with tolerant plants having lower growth rates but higher phosphorus concentrations. The gene for arsenate tolerance is polymorphic in arsenate uncontaminated populations. When phosphorus concentration of tolerant phenotypes was determined in one such population, again tolerants had a higher phosphorus status than non-tolerants. Tolerants also had higher rates of vesicular-arbuscular mycorrhizal (VAM) infection. The ecological implications of these results are that it appears that suppression of the high affinity uptake system, is at least in part, compensated by increased mycorrhizal infection. © 1994 Kluwer Academic Publishers.

Challenging conventional risk assessment with respect to human exposure to multiple food contaminants in food: A case study using maize

Mycotoxins and heavy metals are ubiquitous in the environment and contaminate many foods. The widespread use of pesticides in crop production to control disease contributes further to the chemical contamination of foods. Thus multiple chemical contaminants threaten the safety of many food commodities; hence the present study used maize as a model crop to identify the severity in terms of human exposure when multiple contaminants are present. High Content Analysis (HCA) measuring multiple endpoints was used to determine cytotoxicity of complex mixtures of mycotoxins, heavy metals and pesticides. Endpoints included nuclear intensity (NI), nuclear area (NA), plasma membrane permeability (PMP), mitochondrial membrane potential (MMP) and mitochondrial mass (MM). At concentrations representing legal limits of each individual contaminant in maize (3. ng/ml ochratoxin A (OTA), 1. μg/ml fumonisin B1 (FB1), 2. ng/ml aflatoxin B1 (AFB1), 100. ng/ml cadmium (Cd), 150. ng/ml arsenic (As), 50. ng/ml chlorpyrifos (CP) and 5. μg/ml pirimiphos methyl (PM), the mixtures (tertiary mycotoxins plus Cd/As) and (tertiary mycotoxins plus Cd/As/CP/PM) were cytotoxic for NA and MM endpoints with a difference of up to 13.6% (. p≤. 0.0001) and 12% (. p≤. 0.0001) respectively from control values. The most cytotoxic mixture was (tertiary mycotoxins plus Cd/As/CP/PM) across all 4 endpoints (NA, NI, MM and MMP) with increases up to 61.3%, 23.0%, 61.4% and 36.3% (. p≤. 0.0001) respectively. Synergy was evident for two endpoints (NI and MM) at concentrations contaminating maize above legal limits, with differences between expected and measured values of (6.2-12.4% (. p≤. 0.05-. p≤. 0.001) and 4.5-12.3% (. p≤. 0.05-. p≤. 0.001) for NI and MM, respectively. The study introduces for the first time, a holistic approach to identify the impact in terms of toxicity to humans when multiple chemical contaminants are present in foodstuffs. Governmental regulatory bodies must begin to contemplate how to safeguard the population when such mixtures of contaminants are found in foods and this study starts to address this critical issue.

What defines a geochemical map? Implications for environmental assessment.

The environmental quality of land is often assessed by the calculation of threshold values which aim to differentiate between concentrations of elements based on whether the soils are in residential or industrial sites. In Europe, for example, soil guideline values exist for agricultural and grazing land. A threshold is often set to differentiate between concentrations of the element that naturally occur in the soil and concentrations that result from diffuse anthropogenic sources. Regional geochemistry and, in particular, single component geochemical maps are increasingly being used to determine these baseline environmental assessments. The key question raised in this paper is whether the geochemical map can provide an accurate interpretation on its own. Implicit is the thought that single component geochemical maps represent absolute abundances. However,because of the compositional (closed) nature of the data univariate geochemical maps cannot be compared directly with one another.. As a result, any interpretation based on them is vulnerable to spurious correlation problems. What does this mean for soil geochemistry mapping, baseline quality documentation, soil resource assessment or risk evaluation? Despite the limitation of relative abundances, individual raw geochemical maps are deemed fundamental to several applications of geochemical maps including environmental assessments. However, element toxicity is related to its bioavailable concentration, which is lowered if its source is mixed with another source. Elements interact, for example under reducing conditions with iron oxides, its solid state is lost and arsenic becomes soluble and mobile. Both of these matters may be more adequately dealt with if a single component map is not interpreted in isolation to determine baseline and threshold assessments. A range of alternative compositionally compliant representations based on log-ratio and log-contrast approaches are explored to supplement the classical single component maps for environmental assessment. Case study examples are shown based on the Tellus soil geochemical dataset, covering Northern Ireland and the results of in vitro oral bioaccessibility testing carried out on a sub-set of archived Tellus Survey shallow soils following the Unified BARGE (Bioaccessibility Research Group of Europe).

High-temperature stability study of 1 nm Al2O3 deposited on InAs surfaces investigated by synchrotron radiation based photoemission spectroscopy

High-resolution soft x-ray photoemission spectroscopy (SXPS) has been used to study the high-temperature thermal stability of ultra-thin atomic layer deposited (ALD) Al2O3 layers (~1 nm) on sulfur passivated and native oxide covered InAs surfaces. While the arsenic oxides were removed from both interfaces following a 600 °C anneal, a residual indium oxide signal remained. No significant differences were observed between the sulfur passivated and native oxide surfaces other than the thickness of the interfacial oxide layer while the Al2O3 stoichiometry remained unaffected by the anneals. The energy band offsets were determined for the Al2O3 on the sulfur passivated InAs surface using both valence band edge and shallow core-level photoemission measurements.

Compositonal Analysis of Potentially harmful Elements in Soils: Implications for Epidemiology and Kidney Disease

A substantial proportion of aetiological risks for many cancers and chronic diseases remain unexplained. Using geochemical soil and stream water samples collected as part of the Tellus Project studies, current research is investigating naturally occurring background levels of potentially toxic elements (PTEs) in soils and stream sediments and their possible relationship with progressive chronic kidney disease (CKD). The Tellus geological mapping project, Geological Survey Northern Ireland, collected soil sediment and stream water samples on a grid of one sample site every 2 km2 across the rural areas of Northern Ireland resulting in an excess of 6800 soil sampling locations and more than 5800 locations for stream water sampling. Accumulation of several PTEs including arsenic, cadmium, chromium, lead and mercury have been linked with human health and implicated in renal function decline. The hypothesis is that long-term exposure will result in cumulative exposure to PTEs and act as risk factor(s) for cancer and diabetes related CKD and its progression. The ‘bioavailable’ fraction of total PTE soil concentration depends on the ‘bioaccessible’ proportion through an exposure pathway. Recent work has explored this bioaccessible fraction for a range of PTEs across Northern Ireland. In this study the compositional nature of the multivariate geochemical PTE variables and bioaccessible data is explored to augment the investigation into the potential relationship between PTEs, bioaccessibility and disease data.

Arsénio em águas subterrâneas em Portugal

Da totalidade da água existente na Terra, somente 1% diz respeito à água subterrânea, recurso finito e essencial para a sobrevivência do Homem. A composição química das águas subterrâneas é influência não só pela actividade humana, mas também pelas características químicas do substrato geológico. As rochas e os sedimentos funcionam como meio de transporte e armazém desse tipo de águas e a presença de certos minerais pode originar a contaminação natural das águas subterrâneas em elementos prejudiciais para o Homem. Um desses elementos é o arsénio. Uma vez que a concentração máxima admitida de arsénio para água consumo humano diminuiu dos anteriores 50 mg.l-1 para os actuais 10 mg.l-1,a probabilidade de encontrar concentrações naturais em arsénio em águas subterrâneas acima desse limite aumentou. Este trabalho visa estudar e compreender, através de ensaios laboratoriais, a interacção água/rocha em termos químicos e a mobilidade/comportamento do arsénio em seis zonas de Portugal Continental com contextos geológicos diferentes (Vila Flor – Formação Filito-Quartzítica, Baião – granitos, Cacia – sedimentos do Cretácico, Mamodeiro – sedimentos do Neogénico, Escusa – calcários dolomíticos e Beja - gabros). Para o efeito, nas zonas de estudo mencionadas foram colhidas amostras de rocha ou sedimento e de água subterrânea que foram analisadas para 36 e 76 elementos, respectivamente. A componente mineralógica e as fases suporte do As foram estudadas recorrendo à análise por difracção de raios X, microssonda electrónica e à aplicação da extracção química selectiva sequencial. A mobilização do As foi avaliada através da realização de ensaios de coluna e de agitação com hidrocarbonetos derivados do petróleo. No primeiro ensaio, a circulação de diferentes soluções com diferentes velocidades lineares no interior de colunas de vidro cheias de rocha moída, avaliou a presença de As associado a fases hidrossolúveis e biodisponíveis. No segundo, a agitação de rocha moída com água e hidrocarbonetos derivados do petróleo pretendeu avaliar o comportamento do As quando um aquífero apresenta uma contaminação com aquele tipo de hidrocarbonetos.

Assessment of biocompatibility of selected ferroelectric ceramics

Desde há muitas décadas que é sabido que os organismos vivos, em especial os tecidos, reagem fisicamente a estímulos eléctricos, podendo esses efeitos reproduzirem-se numa libertação de químicos endógenos, ou deformar a sua estrutura física. O tecido ósseo por si só é considerado um material/tecido piezoeléctrico, deformando-se mecanicamente quando lhe é induzido um estímulo eléctrico e vice-versa, ou seja, produz um potencial eléctrico quando sofre uma tracção ou compressão mecânica. A hipótese de que um material ferroeléctrico possa vir a produzir efeitos no desempenho deste tipo de tecidos é então proposta, como por exemplo, para uma melhor, mais rápida e eficaz regeneração óssea. Estes mesmos materiais ferroeléctricos podem porventura alterar as cargas de superfície dos tecidos vivos de modo a atrair, atrasar ou até impedir o fluxo iónico de elementos químicos específicos responsáveis pelo processo de regeneração. São escolhidos então o niobato de lítio e o tantalato de lítio como cerâmicos ferroeléctricos e foi estudada pela primeira vez a sua bioactividade in vitro, esperando-se encontrar pistas relativas à sua bioactividade in vivo. Estes cerâmicos ferroeléctricos foram seleccionados devido às suas importantes propriedades piezoeléctricas e ferroeléctricas. Estas propriedades podem abrir um novo e importante leque de aplicações biomédicas caso estes cerâmicos sejam bioactivos. Este trabalho foi dividido em 3 fases: (i) sintetização dos pós de niobato de lítio e tantalato de lítio, (ii) caracterização dos pós e (iii) preparação das amostras e (iv) estudo da bioactividade destes cerâmicos ferroeléctricos. Os pós foram produzidos através de um processo simples de mistura/moagem seguido de calcinação. Foram estudadas as fases cristalinas presentes através de Difracção de raios-X (DRX) e avaliadas as características morfológicas destes pós, nomeadamente o diâmetro de partículas e área superficial específica. De modo a simular o ambiente do plasma humano, foi produzido sinteticamente um “Simulated Body Fluid” (SBF). Seguidamente as amostras foram imersas nesse ambiente líquido por 1, 3, 7, 15 e 21 dias. Após remoção dos pós foram realizadas uma série de análises de modo a estudar a sua bioactividade. De entre estes testes destacam-se a microscopia electrónica de varrimento (SEM/EDS), DRX e espectroscopia de Infravermelho por transformada de Fourier com reflectância total atenuada (FTIR-ATR). Embora não tenham sido detectadas alterações no DRX realizado aos pós, verificou-se a formação de aglomerados de fosfato de cálcio na superfície dos pós através do SEM, resultados estes, reforçados pelo EDS e FTIR-ATR. Estes precipitados de fosfato de cálcio indiciam a capacidade destes pós cerâmicos ferroeléctricos se comportarem como bioactivos em contacto com tecidos ósseos in vivo.

Aplicação de cortiça em dois tipos de reatores para tratamento de água

A qualidade da água degradou-se de forma relevante nas últimas décadas e os processos de sorção têm vindo a ser investigados como métodos promissores para o tratamento de águas contaminadas. Neste trabalho avaliou-se a capacidade de dois tipos de cortiça para a remoção de diversos contaminantes, em reatores de vaso fechado e de leito fixo. Os ensaios realizados em reatores de vaso fechado permitiram (i) avaliar o efeito do pH e da granulometria na eficiência dos sorventes na remoção de mercúrio e (ii) avaliar a afinidade dos sorventes para outros contaminantes, nomeadamente arsénio, cádmio, níquel e chumbo. Estruturalmente as duas cortiças estudadas aparentam ser semelhantes, com uma pequena diferença de comportamento ácido-base e não apresentam diferenças estatisticamente significativas na remoção de mercúrio. Os resultados obtidos permitiram constatar que o processo de remoção é independente do pH, tendo-se obtido percentagens de remoção da ordem dos 80% e de concentrações de mercúrio na cortiça na ordem dos 117 μg/g. As cortiças estudadas revelaram-se menos eficazes no tratamento de água com os restantes contaminantes, atingindo percentagens de remoção máximas de 0% para As, 11% para Cd, 35% para Ni e 69% para Pb. Os ensaios em leito fixo, mesmo sem terem sido otimizados, revelam que é possível obter uma eficácia de remoção de mercúrio superior a 90% nas primeiras 40 horas de trabalho, sendo a concentração de mercúrio no leito de 680 μg/g. Relativamente aos mecanismos de sorção, os resultados experimentais indicam que estes são possivelmente de natureza química e que as interações eletrostáticas têm pouca importância.

Metais em águas e sedimentos da plataforma dos Açores

A presente tese tem por objetivo principal contribuir para o conhecimento da geoquímica sedimentar da zona oceânica da crista da Terceira e montanhas submarinas a sul (região entre 29-39ºN e 27-32ºW), integrando também a caraterização dos metais e nutrientes na coluna de água e propondo concentrações para servirem de referência nesta região do Atlântico Central. Para o efeito foram realizadas amostragens na coluna de água em sete locais e de sedimento em cinco locais, durante a campanha oceanográfica designada por EMEPC/AÇORES/G3/2007 a bordo do navio SV Kommandor Jack, no âmbito do projeto da Estrutura de Missão para a Extensão da Plataforma Continental (EMEPC). Os perfis de CTD da coluna de água na região estudada revelam a presença de massas de água distintas: a Western North Atlantic Central Water (WNACW), a Eastern North Atlantic Central Water tropical (ENACWt), a Eastern North Atlantic Central Water polar (ENACWp), a Mediterranean Overflow Water (MOW), a Deep Mediterranean Water (DMW) e a North Eastern Atlantic Deep Water (NEADW). Observou-se nos perfis de temperatura e salinidade, referentes aos primeiros 200 m da coluna de água, um gradiente meridional negativo entre as estações localizadas na crista da Terceira e as estações localizadas mais a sul. Observou-se nas águas superficiais valores de oxigénio dissolvido de 93% e de pH de 8,1, assim como que as concentrações dos nutrientes NOx, PO4 e SiO2 variam de acordo com a atividade biológica, tendo-se registado concentrações medianas mais baixas, respetivamente de 6,5, 0,23 e 1,3 mol L-1, que aumentam com a profundidade devido à ausência de produção primária (respetivamente 31, 1,4 e 22 mol L-1). As concentrações de NH4 e de SO4 não variam significativamente nas massas de água, sendo os valores medianos mínimos e máximos de 0,69 a 0,79 mol L-1 para o NH4 e de 30 a 32 mol L-1 para o SO4. São propostas concentrações de referência para as massas de água, para os elementos cobre, cádmio, chumbo e arsénio. Os perfis de sedimento analisados permitem distinguir os sedimentos na crista da Terceira (core A) dos restantes (cores B a E). A grande variabilidade textural encontrada no core A, que contrasta com os outros cores analisados, deve-se a importantes contribuições terrígenas, originadas pela erosão sub-aérea e pela atividade vulcânica das ilhas próximas. iv resumo (continuação) A análise mineralógica, efetuada à fração areia e à fração fina (< 63 μm), confirma que os sedimentos do core A derivam de rochas vulcânicas formadas maioritariamente por piroxenas, olivinas, anfíbolas, biotite, alterites e ainda calcite, plagióclase e magnetite, tendo-se identificado ao microscópio a glauconite e o vidro vulcânico. De acordo com a composição química destes minerais o core A apresenta valores mais elevados de Al, Fe, K, P, Mg, Si, Na, Zn, V, Cr e Mn relativamente aos cores B a E. Os cores B a E apresentam grandes quantidades de calcite (>80%) formada maioritariamente por foraminíferos e nanoplâncton calcário (cocolitóforos). A fração areia confirma a composição maioritariamente carbonatada com grande abundância de material biogénico formado por oozes de foraminíferos (planctónicos e bentónicos) com raras espículas de espongiários e restos de conchas. Os cores B a E apresentam valores muito mais elevados que o core A para os elementos Ca e Sr. Os resultados para o Al, Fe, K, P, Si, Na, As, Cu, Ni, Zn, V, Cr, Li, Pb, Cd e Co presentes nos locais B, C, D e E sugerem que estes cores são comparáveis aos sedimentos de fundo carbonatados. Propõe-se concentrações de referência para a região do Atlântico compreendida entre 29-39ºN e 27-32ºW considerando a primeira camada colhida em cada core. Para o core A as concentrações são normalizadas a 5% de Al e CaCO3, enquanto que para os cores B a E são normalizadas a 2% de Al e CaCO3. Assim as concentrações de referência para o core A são: As – 18 mg kg-1, Cr – 91 mg kg-1, Cu – 127 mg kg-1, Ni – 84 mg kg-1, Pb – 41 mg kg-1, Hg – 41 ng g-1 e Zn – 482 mg kg-1. Para os cores B a E as concentrações de referência são: As – 3 mg kg-1, Cr – 10 mg kg-1, Cu – 36 mg kg-1 Ni – 12 mg kg -1, Hg – 3 ng g-1 e Zn – 20 mg kg-1. Para os restantes metais as concentrações de referência para o core A são: Al – 9%, Si – 25%, Fe – 6%, Ca – 13%, K – 2%, Mg – 2%, Na – 3%, P – 0,4%, Sr – 900 mg kg-1, Li – 10 mg kg-1, Mn – 1200 mg kg-1, Ba – 700 mg kg-1 e V – 140 mg kg-1. Para os cores B a E as concentrações de referência são: Al – 0,9%, Si – 2%, Fe – 0,2%, Ca – 95%, K – 0,3%, Mg – 0,4%, Na – 0,3%, P – 0,04%, Sr – 2600 mg kg-1, Li – 5 mg kg-1, Mn – 240 mg kg-1, Ba – 345 mg kg-1, Co – 2 mg kg-1 e V – 6 mg kg-1. Os resultados da presente tese constituem um contributo para a caraterização geoquímica da região e podem servir de referência à monitorização futura do mar dos Açores e montes submarinos a sul.

Severe plastic deformation of Al–Zn alloys

In this work, the R&D work mainly focused on the mechanical and microstructural analysis of severe plastic deformation (SPD) of Al–Zn alloys and the development of microstructure–based models to explain the observed behaviors is presented. Evolution of the microstructure and mechanical properties of Al–30wt% Zn alloy after the SPD by the high–pressure torsion (HPT) has been investigated in detail regarding the increasing amount of deformation. SPD leads to the gradual grain refinement and decomposition of the Al–based supersaturated solid solution. The initial microstructure of the Al–30wt% Zn alloy contains Al and Zn phases with grains sizes respectively of 15 and 1 micron. The SPD in compression leads to a gradual decrease of the Al and Zn phase grain sizes down to 4 microns and 252 nm, respectively, until a plastic strain of 0.25 is reached. At the same time, the average size of the Zn particles in the bulk of the Al grains increases from 20 to 60 nm and that of the Zn precipitates near or at the grain boundaries increases as well. This microstructure transformation is accompanied at the macroscopic scale by a marked softening of the alloy. The SPD produced by HPT is conducted up to a shear strain of 314. The final Al and Zn grains refine down to the nanoscale with sizes of 370 nm and 170 nm, respectively. As a result of HPT, the Zn–rich (Al) supersaturated solid solution decomposes completely and reaches the equilibrium state corresponding to room temperature and its leads to the material softening. A new microstructure–based model is proposed to describe the softening process occurring during the compression of the supersaturated Al–30wt% Zn alloy. The model successfully describes the above–mentioned phenomena based on a new evolution law expressing the dislocation mean free path as a function of the plastic strain. The softening of the material behavior during HPT process is captured very well by the proposed model that takes into consideration the effects of solid solution hardening and its decomposition, Orowan looping and dislocation density evolution. In particular, it is demonstrated that the softening process that occurs during HPT can be attributed mainly to the decomposition of the supersaturated solid solution and, in a lesser extent, to the evolution of the dislocation mean free path with plastic strain.

Caracterização endócrina da PTH-L e calcitonina no transporte de cálcio e na secreção de bicarbonato no intestino da dourada (Sparus auratus)

Dissertação de Mestrado, Biologia Marinha, Faculdade de Ciências do Mar e do Ambiente, Universidade do Algarve, 2009